Project WILAS – West Iberia Lithosphere and Astenosphere Structure
Autor(a) principal: | |
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Data de Publicação: | 2011 |
Outros Autores: | , , , , , |
Tipo de documento: | Artigo de conferência |
Idioma: | por |
Título da fonte: | Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
Texto Completo: | http://hdl.handle.net/10174/3558 |
Resumo: | The lithosphere of Iberia has been formed through a number of processes of continental collision and extension: in Lower Paleozoic, the collision of three tectonics blocks produced the Variscan Orogeny, the main event of formation of the lithosphere. The subsequent Mesozoic rifting and breakup of the Pangea had a profound effect on the continental crust of Iberia. Since the Miocene, the southern interaction between Africa and Iberia is characterized by a diffuse convergent margin that originates a vast area of deformation. The impact of this complex tectonic in the structure of the Lithosphere remains an incognito, especially in its western part. Project WILAS (PTDC/CTE-GIX/097946/2008) is a 3 years project funded by FCT in which a temporary network of more than 20 BB seismic stations is being deployed in Portugal between 2010-2012. It will extend to the western border of Iberia the coverage of the TOPO-IBERIA project. The project aims to image the 3D structure beneath W Iberia. The knowledge of the Crust, Lithosphere and Astenosphere seismic structure must be dealt at different scales, involving different but complementary methods. |
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Project WILAS – West Iberia Lithosphere and Astenosphere StructureSismicidadeRedes sísmicasEstrutura da Crusta PortuguesaTomografia SismicaThe lithosphere of Iberia has been formed through a number of processes of continental collision and extension: in Lower Paleozoic, the collision of three tectonics blocks produced the Variscan Orogeny, the main event of formation of the lithosphere. The subsequent Mesozoic rifting and breakup of the Pangea had a profound effect on the continental crust of Iberia. Since the Miocene, the southern interaction between Africa and Iberia is characterized by a diffuse convergent margin that originates a vast area of deformation. The impact of this complex tectonic in the structure of the Lithosphere remains an incognito, especially in its western part. Project WILAS (PTDC/CTE-GIX/097946/2008) is a 3 years project funded by FCT in which a temporary network of more than 20 BB seismic stations is being deployed in Portugal between 2010-2012. It will extend to the western border of Iberia the coverage of the TOPO-IBERIA project. The project aims to image the 3D structure beneath W Iberia. The knowledge of the Crust, Lithosphere and Astenosphere seismic structure must be dealt at different scales, involving different but complementary methods.APMG- Associação Portuguesa de Meteorologia e Geofísica2012-01-16T09:58:17Z2012-01-162011-01-01T00:00:00Zinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/conferenceObjecthttp://hdl.handle.net/10174/3558http://hdl.handle.net/10174/3558porsimnaonaondndndndndbafcc@uevora.ptnd249Dias, NunoCarrilho, FernandoHaberland, C.Fonseca, J.Custódio, S.Caldeira, BentoVillaseñor, Ainfo:eu-repo/semantics/openAccessreponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãoinstacron:RCAAP2024-01-03T18:40:55Zoai:dspace.uevora.pt:10174/3558Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireopendoar:71602024-03-20T00:59:02.848881Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãofalse |
dc.title.none.fl_str_mv |
Project WILAS – West Iberia Lithosphere and Astenosphere Structure |
title |
Project WILAS – West Iberia Lithosphere and Astenosphere Structure |
spellingShingle |
Project WILAS – West Iberia Lithosphere and Astenosphere Structure Dias, Nuno Sismicidade Redes sísmicas Estrutura da Crusta Portuguesa Tomografia Sismica |
title_short |
Project WILAS – West Iberia Lithosphere and Astenosphere Structure |
title_full |
Project WILAS – West Iberia Lithosphere and Astenosphere Structure |
title_fullStr |
Project WILAS – West Iberia Lithosphere and Astenosphere Structure |
title_full_unstemmed |
Project WILAS – West Iberia Lithosphere and Astenosphere Structure |
title_sort |
Project WILAS – West Iberia Lithosphere and Astenosphere Structure |
author |
Dias, Nuno |
author_facet |
Dias, Nuno Carrilho, Fernando Haberland, C. Fonseca, J. Custódio, S. Caldeira, Bento Villaseñor, A |
author_role |
author |
author2 |
Carrilho, Fernando Haberland, C. Fonseca, J. Custódio, S. Caldeira, Bento Villaseñor, A |
author2_role |
author author author author author author |
dc.contributor.author.fl_str_mv |
Dias, Nuno Carrilho, Fernando Haberland, C. Fonseca, J. Custódio, S. Caldeira, Bento Villaseñor, A |
dc.subject.por.fl_str_mv |
Sismicidade Redes sísmicas Estrutura da Crusta Portuguesa Tomografia Sismica |
topic |
Sismicidade Redes sísmicas Estrutura da Crusta Portuguesa Tomografia Sismica |
description |
The lithosphere of Iberia has been formed through a number of processes of continental collision and extension: in Lower Paleozoic, the collision of three tectonics blocks produced the Variscan Orogeny, the main event of formation of the lithosphere. The subsequent Mesozoic rifting and breakup of the Pangea had a profound effect on the continental crust of Iberia. Since the Miocene, the southern interaction between Africa and Iberia is characterized by a diffuse convergent margin that originates a vast area of deformation. The impact of this complex tectonic in the structure of the Lithosphere remains an incognito, especially in its western part. Project WILAS (PTDC/CTE-GIX/097946/2008) is a 3 years project funded by FCT in which a temporary network of more than 20 BB seismic stations is being deployed in Portugal between 2010-2012. It will extend to the western border of Iberia the coverage of the TOPO-IBERIA project. The project aims to image the 3D structure beneath W Iberia. The knowledge of the Crust, Lithosphere and Astenosphere seismic structure must be dealt at different scales, involving different but complementary methods. |
publishDate |
2011 |
dc.date.none.fl_str_mv |
2011-01-01T00:00:00Z 2012-01-16T09:58:17Z 2012-01-16 |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/conferenceObject |
format |
conferenceObject |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
http://hdl.handle.net/10174/3558 http://hdl.handle.net/10174/3558 |
url |
http://hdl.handle.net/10174/3558 |
dc.language.iso.fl_str_mv |
por |
language |
por |
dc.relation.none.fl_str_mv |
sim nao nao nd nd nd nd nd bafcc@uevora.pt nd 249 |
dc.rights.driver.fl_str_mv |
info:eu-repo/semantics/openAccess |
eu_rights_str_mv |
openAccess |
dc.publisher.none.fl_str_mv |
APMG- Associação Portuguesa de Meteorologia e Geofísica |
publisher.none.fl_str_mv |
APMG- Associação Portuguesa de Meteorologia e Geofísica |
dc.source.none.fl_str_mv |
reponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação instacron:RCAAP |
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Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação |
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RCAAP |
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RCAAP |
reponame_str |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
collection |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
repository.name.fl_str_mv |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação |
repository.mail.fl_str_mv |
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1799136473041076224 |